Irving Nature Park

Take exit 119A off of Highway 1 towards Bleury Street. You will come to an intersection and turn right onto Sand Cove Road. You will follow this road all the way to the park. There is a sand park that you can follow to arrive at the main parking area and even continue your drive through the park!

The geology of the Irving Nature Park includes both Devonian to Carboniferous bedrock (359 to 346 million years old) exposed on Taylors Island and at Sheldon Point and overlying sand, gravel and clay deposited during the last ice age less than 15,000 years ago. The age of the older volcanic and sedimentary rocks has been hard to determine.

Although they have many interesting features, this note will focus on the ice age geology of the Irving Nature Park. This is one of the best places in Stonehammer to see this part of the geologic record. The ice age geology is made up of “unconsolidated” sediments. They are not rock yet, they are too young.

The end of the ice age was a time of rapid climate change especially during the “Younger Dryas” cold interval. About 11,000 years ago temperatures plummeted about 7˚C in a decade. Sub-arctic insects re-invaded the Maritimes for hundreds of years until temperature warmed again. A peat bog on the hill at Saints Rest Beach records this rapid climate event.

At a time geologists call the “Last Glacial Maximum”, about 20,000 years ago, continental glaciers covered most of North America, including the Maritimes. By 10,000 years ago New Brunswick was probably “ice-free”. As the glaciers retreated they left piles of sand and gravel along their margin. Called “moraines” and “outwash”, these piles of sediment are easily seen on the modern landscape. We often use them as sand and gravel quarries. The quarry on Sand Cove Road above the beach is an example. About 15,000 years ago the front of the glacier stood here at the Irving Nature Park. It is called a tidewater glacier since the glacier ice was up against the ocean. The red clay along the beach cliffs is composed of layers of ocean sediment. Occasionally fossils of snails, clams, sea urchins and starfish can be found in the clay. As the glacier continued to retreat it left a series of moraines where it stood still for a period of time. Looking northwest from the beach you can see Manawagonish Road on the hill. The road is built on the Manawagonish Moraine. This moraine acted as a dam and forced the St. John River to flow through the Reversing Falls.

The natural Landscape at the Irving Nature Park is spectacular. Although, Saints Rest marsh has a complicated history. Dyked by the Acadians sometime between 1786 and 1864 the marsh was first managed mainly for pasture and hay production. Barns were constructed in the marsh, roads traversed it, and forestry and gravel extraction occurred in the adjacent upland and beach. Sometime prior to WWII the marsh was greatly modified as a military shooting range. Subsequent abandonment in the 1950’s resulted in the dyke falling into disrepair and eventually being breached. Now, the largest salt marsh in Saint John, Saints Rest is part of the Irving Nature Park.

For more information click here.

Manawagonish Island Nature Preserve, Saints Rest Marsh, F. Gordon Carvell Nature Preserve, Sheldon Point trailhead, McClarens Beach, Bayshore Beach, Carleton Martello Tower.